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2020 GCSSEPM Foundation Perkins-Rosen Research Conference

The Cenomanian-Turonian Stratigraphic Interval Across the Americas: Argentina to Alaska

The Cenomanian-Turonian stratigraphic interval is highly significant, both scientifically and economically. Its importance derives from the fact that fine-grained sediments of this age are commonly unusually enriched in organic carbon, it hosts a dramatic carbon isotopic excursion (Oceanic Anoxic Event—OAE-2) and its deposition was coincident with some of highest sea levels in Phanerozoic Earth History. C-T intervals are both rich source rocks for conventional hydrocarbon accumulations as well as serving as prolific reservoirs for unconventional hydrocarbon production.

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